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Landscape Development - Gouverneur Central School District
Landscape Development - Gouverneur Central School District

... Gradient (slope) – a way to describe the land because it is a measurable characteristic and useful because it shows the development of soils The three major types of landscapes are distinguished by gradient, elevation, and rock structure. ESRT page 2. They are: 1. Mountains: high elevation, non-sedi ...
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Chapter 3 Weathering, Soil, and Mass Wasting

... • http://ruby.colorado.edu/~smyth/G1010-06.html http://www.geo.lsa.umich.edu/~crlb/COURSES/117-IntroductiontoGeology/Lec28/lec28.html ...
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Rock Cycle Weathering Vocab

... soil that can be distinguished from the layers above and below it; also a boundary between two rock layers that have different physical properties the surface layer of the soil, which is usually richer in organic matter than the subsoil is ...
soil horizons
soil horizons

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File

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Sedimentary Rocks

... Sedimentary Rock - Sediment – small pieces or fragments of weathered rock - Wide range of sizes of particles  Smaller than sand to larger than a car  Generally pebble size and smaller is meant by the term sediment ...
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... 13) _____ The picking up and removal of rock pieces and other particles. 14) _____ The dropping off of eroded particles in different locations from where they were picked up. 15) _____ A mixture of weathered rock, air, water, and humus that can support the growth of rooted plants. 16) _____ Decayed ...
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... stays the same no matter how small the piece of rock; frost wedging Chemical weathering = rock composition CHANGES from one form to another; water dissolving limestone ...
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Factors that Shape the Earth

... Weathering breaks down rock into small pieces; erosion is the process that picks up those pieces and carries them away. Deposition drops them off in new locations. The presence of plants reduces the amount of soil erosion because roots hold water and soil in place. Agents of erosion: Rivers -- rain ...
Chapter 23 test - Geneva Area City Schools
Chapter 23 test - Geneva Area City Schools

... Completion Complete each statement. 20. ____________________ is the process by which rocks are chemically altered or physically broken down into fragments at or near Earth’s surface. 21. The main agent of chemical weathering is ____________________. 22. Deposits of windblown dust are called _______ ...
Erosion Notes and Fill in the Blank HW
Erosion Notes and Fill in the Blank HW

... ________________ occurs. Soil is a mixture of: rock particles, minerals, decayed _______________ matter, water and air. Soil forms as rock is broken down by _________________ and mixes with other materials on the surface. EROSION NOTES 1. ________________ and _______________ Forces wear down and bu ...
Quiz 5 - Brooklyn College
Quiz 5 - Brooklyn College

... 7. As soon as a rock particle (loosened by the weathering processes) is transported somewhere else, that process is called __________. o ...
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Weathering



Weathering is the breaking down of rocks, soil and minerals as well as artificial materials through contact with the Earth's atmosphere, biota and waters. Weathering occurs in situ, roughly translated to: ""with no movement"" , and thus should not be confused with erosion, which involves the movement of rocks and minerals by agents such as water, ice, snow, wind, waves and gravity and then being transported and deposited in other locations.Two important classifications of weathering processes exist – physical and chemical weathering; each sometimes involves a biological component. Mechanical or physical weathering involves the breakdown of rocks and soils through direct contact with atmospheric conditions, such as heat, water, ice and pressure. The second classification, chemical weathering, involves the direct effect of atmospheric chemicals or biologically produced chemicals also known as biological weathering in the breakdown of rocks, soils and minerals. While physical weathering is accentuated in very cold or very dry environments, chemical reactions are most intense where the climate is wet and hot. However, both types of weathering occur together, and each tends to accelerate the other. For example, physical abrasion (rubbing together) decreases the size of particles and therefore increases their surface area, making them more susceptible to rapid chemical reactions. The various agents act in concert to convert primary minerals (feldspars and micas) to secondary minerals (clays and carbonates) and release plant nutrient elements in soluble forms.The materials left over after the rock breaks down combined with organic material creates soil. The mineral content of the soil is determined by the parent material, thus a soil derived from a single rock type can often be deficient in one or more minerals for good fertility, while a soil weathered from a mix of rock types (as in glacial, aeolian or alluvial sediments) often makes more fertile soil. In addition, many of Earth's landforms and landscapes are the result of weathering processes combined with erosion and re-deposition.
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